KMS Technologies KJT Enterprises Inc.

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1 KMS Technologies KJT Enterprises Inc.

2 Vision Products To make electromagnetics (EM) in general & time domain controlled source electromagnetics (tcsem ) in particular a routine tool in hydrocarbon exploration & production fully integrated with seismic. To carry the technology to monitoring of water & steam-flooding of hydrocarbon reservoirs and production monitoring of geothermal reservoirs. This is achieved via installation of permanent arrays. Our products support borehole, land and marine real-time applications. Our services complement our technology offerings. All about EM KMS Technologies focuses on advanced electromagnetic methods for the oil/geothermal industry to increase the discovery & recovery factors or carry out production monitoring. We support our tehnology via high-quality services, state-of-the-art R&D projects, several unique hardware & software products. Microseismic / Electromagnetic monitoring system Wireless acquisition systems Magnetotellurics: DC to 40 khz, 24 & 32 bit; true array functionality (wireless) Surface-to-borehole EM Custom marine systems Mud logging (porosity & permeability) with NMR Transmitters Land 100 kva or 150 kva Transition zone Marine (custom) Sensors Magnetometers (DC to 200 khz) Electrodes Services Heavy oil & water flood monitoring - 3D feasibility - Pilot demonstration - Technology transfer 3D modeling - MT Interpretation - Feasibility studies - CSEM interpretation EM demonstration & training surveys 2016 KMS Technologies - KJT Enterprises Inc. V 2.5 Page 1 of 15

3 Fluxgate & search coil magnetometers Wide-band Magnetotelluric (MT) system The next generation wide band system comprises a portable KMS-820 data acquisition unit: KMS-820 features (land-marine-borehole) Low-power design to increase battery life Long range capability (up to 5 miles line-of-sight or unlimited distance in mesh network mode) WIFI (server or point-to-point) Bandwidth: DC-40 khz Up to 80 khz sampling rate Six 24-bit GPS synchronized channels & unlimited 32 bit channels Low noise channels Customizable digital interface for digital sensors & other devices Portable & lightweight The Laboratory of Electromagnetic Innovations (LEMI) was founded 2008 as a joint venture between KMS Technologies & the Lviv Centre of Institute for Space Research (LCISR) to focus on the development & production of high quality electromagnetic (EM) sensors. LEMI is located in Lviv, Ukraine KMS Technologies - KJT Enterprises Inc. V 2.5 Page 2 of 15

4 Microseismic & Electromagnetic Array data acquisition system Product overview Main components Land KMS-820 data acquisition unit KMS bit interface module LEMI-701 non-polarizable, lead-free electrodes LEMI-120 induction coil sensor ( ,000 Hz) LEMI-118 induction coil sensor (1 70,000 Hz) KMS-029 fluxgate magnetic sensor 32-bit, (DC 180 Hz) Multicomponent geophones Marine KMS-870 broad-band seismic/em marine deep-water node The KMS Array data acquisition system is developed for EM (ElectroMagnetic) and micro-seismic applications to obtain subsurface resistivity and velocity structure for oil and gas exploration. It also can be used in general purpose acquisition and long term monitoring services. The system comes with various options to facilitate microseismic and electromagnetic reservoir monitoring. It also synchronizes and integrates with our borehole acquisition system and our marine MT acquisition node (KMS-870). The core of the system is the KMS-820 Data Acquisition Unit which has six 24-bit low noise, low drift analog channels and, through the digital port, and the KMS-831, unlimited channel expansion. Typically, the digital port is used to record 32- bit fluxgate magnetic fields, at the same time as acquiring coils. The 24-bit architecture goes to 100 KHz sampling, and the 32-bit architecture to Hz. All channels are sampled simultaneously and synchronized with GPS. In addition, the KMS-820 can be used to control the KMS-500 marine or the KMS-5100 land transmitter. Multiple communication and data harvesting options exist: USB cable, SD card exchange, long range wireless, WIFI via router (when available), and WIFI point-to-point direct connections. LAN is optional. All EM methods can also be run on a seismic crew. A variety of survey configurations, from single recording station to 3D acquisition arrays are possible. Optional KMS-5100 land transmitter KMS-500 transition zone transmitter 3D software sales & interpretation services System highlights: Acquire microseismic data independently or simultaneously with EM Combined CSEM & natural source EM acquisition in one receiver deployment Same layout can acquire different methods by adding optional transmitters or geophones Combined MT/AMT measurements to give high resolution mapping and great depth MT: Fully synchronized SIMULTANEOUS acquisition for ultra-low frequencies (KMS-029: DC-180 Hz), standard MT band (LEMI-120: Hz), AMT band (LEMI-118>: 1 50,000 Hz) Lightweight, portable, rugged, low power consumption Wireless network (long range), GPS synchronized, wide bandwidth & dynamic range 24-bit or 32-bit digital resolution, DC to 50 khz signal bandwidth Low cost with large channel count (unlimited) Efficient field operations with or without cables Each KMS-820 can be expanded to unlimited channels with multiple KMS-831 (32-bit) High sampling rate to adapt to various geophysical methods (24-bit to 80 khz, 32-bit to 4 khz) info@kmstechnologies.com KMS Technologies - KJT Enterprises Inc. V 2.5 Page 3 of 15

5 KMS-820 Array System - Main components 1. KMS-820 digital acquisition system 2. KMS-831 sub-acquisition controller 3. KMS-029 (fluxgate magnetometer) 4. LEMI-120 (low frequency magnetometer) 5. LEMI-118 (low frequency magnetometer) 6. LEMI-701 electrode 7. S-20 (air coil magnetic sensor) 8. Multicomponent geophone 9. Misc. interconnect cables 10. Accessories (KMS-300, USB cable) 11. Laptop computer 11A KMS-410 Lithium Ion batteries 12. KMS-5100 transmitter (not to scale) Single receiver station layout (example only) The KMS array data acquisition system allows great flexibility in acquisition design adjusting with survey requirements, including that all receiver stations may not be identical. The acquisition scheduler allows the system to be used for different acquisitions and even method in one drop. The figure below shows a sample layout only, purely to illustrate how a receiver station might be configured KMS Technologies - KJT Enterprises Inc. V 2.5 Page 4 of 15

6 KMS-820 KMS-831 KMS-029 E-field electrodes. Ex and Ey Magnetometer coils. Hx, Hy, Hz Multicomponent geophone 3 axis fluxgate magnetometer Applications Reservoir monitoring Oil and gas exploration (land & marine) Hydrocarbon reservoir dynamics & CO2 storage monitoring Porosity mapping within carbonate reservoirs Geothermal exploration & induced seismicity monitoring Engineering & environmental studies Earthquake prediction research Deep crustal research Metals and mineral exploration Integration to reservoir via borehole (KMS-borehole system) EM methods & microseismics For magnetotellurics (MT) one often uses single site or remote reference recording as shown below. MT, AMT: Magnetotellurics and Audio MT are used for basin reconnaissance and structure studies including near surface applications, mostly oil &gas and geothermal applications. CSAMT: Controlled Source Audio MT uses a transmitter to get better Signal-to-Noise (S/N) ratios for detailed structure investigations of the upper 2 km. TFEM, IP: Time-Frequency Domain ElectroMagnetics and Induced Polarization combine time and frequency domain electromagnetics for hydrocarbon and mineral exploration. (He et al., 2015) LOTEM: Long Offset Transient ElectroMagnetics is applied to detailed structural investigations of the upper 5 km for hydrocarbon and geothermal Exploration & Production. Focused TEM is also possible. (Strack and Pandey, 2007) All EM methods can be combined with simultaneous microseismic acquisition, The KMS-870 includes broadband microseismic and marine MT acquisition in one unit KMS Technologies - KJT Enterprises Inc. V 2.5 Page 5 of 15

7 3D EM/seismic array layouts KMS acquisition systems can be used for large scope 3D EM survey with densely spaced electric sensors and sparsely installed magnetometers. The system s wireless network feature makes field operations very efficient when conducting massive 3D EM survey. Depending upon distance between sites, KMS-820 or KMS-831 with digital interconnect ( 100 m) can be used. KMS-831 is about 5 times less expensive than the KMS-820 and connects to a KMS-820. The figure below shows a layout where on the right you have 3D acquisition using bins where only one site in the bin has all the magnetic sensors. The rest has only electric fields. The center shows mountainous operation for complex terrain which has portable site and can even be helicopter assisted. On the left are 2D lines where each site has the full sensor component set. When running MT on as seismic crew, you usually run the MT site ahead or after the seismic line to avoid operations related noise on the MT data. With CSEM you have multiple option between moving receiver and/or transmitter. Since the CSEM operations are busy you might want to run it after the seismic line. Controlled source transmitter can be added to this at desired locations. KMS team as part of a seismic crew in Brazil acquiring MT data. System configuration table Following table shows the various system configuration options for different surveys and applications. System components can be mixed and matched in a modular fashion. Seismic sensors can be added to each configuration. Each configuration is expandable by adding more KMS-831 sub-acquisition controller. NEW 2016: shallow borehole seismic/em receiver KMS KMS Technologies - KJT Enterprises Inc. V 2.5 Page 6 of 15

8 Reservoir monitoring layout Reservoir monitoring has many different options. Since the reservoir changes are always 3D, careful design is required and multiple transmitter must be used to understand the 3D effects. We use at least two transmitters. Below are examples of the CSEM transmitters, receivers and a sample layout. (Colombo et al., 2010; Hu et al., 2008; Strack, 2010). KMS recommends to carry out a 3D modeling Feasibility including and on-site noise test as FIRST STEP. Below on the right is a typical noise test sensors layout in the field. Survey layouts are usually design as per specific objectives. The example figure shows a layout for water-flood monitoring. The transmitters in this case are not shown. You may add the Shallow Borehole Tool to the receiver sites KMS Technologies - KJT Enterprises Inc. V 2.5 Page 7 of 15

9 MT applications Magnetotellurics (MT) and Audio MT (AMT) target different depth of investigation in hydrocarbon and geothermal exploration. For hydrocarbon exploration, high resistivity lithology such as salt, basalt, and over thrusting often mask underlying sediments. They are difficult to image with seismic data due to high velocities and diffuse scattering. But they can be easily imaged by MT or Lotem method because of their associated large resistivity contrasts. MT utilizes natural variations in the Earth s magnetic field as a source. Natural MT signals come from a variety of induced currents caused by thunderstorms and the ionosphere. The frequency ranges of MT data spans from Hz to 1000 Hz and for AMT from 10 Hz to 20 khz. MT is usually used to map conductive zones like geothermal zones or sediment packages. To map resistors like hydrocarbon reservoir you must use a grounded dipole transmitter (Passalacqua, 1983; Strack et al., 1889), which means you use Controlled Source ElectroMagnetics. For large site count 2D and 3D MT or AMT surveys, the array configuration is more cost effective. The central control unit of the array is capable of controlling several thousand recording units wirelessly. Standard distances are 5 miles without and principally unlimited with wireless relays. Commercial benefits: 2D or 3D MT survey configurations Low cost for 2D or 3D MT and AMT surveys High speed sampling rate allow acquiring MT & AMT data with the same unit Fast and easy operation & deployment of multiple units Customized wireless system for remote system monitoring Designed for dense acquisition spacing for data redundancy & high resolution data recording After Buehnemann et. al., 2002 Time-Frequency ElectroMagnetics (TFEM) applies the Transient ElectroMagnetic (TEM) & Induced Polarization (IP) techniques. It records broad-band frequency & time domain following a scheduled process. An anomaly with the combination of high resistivity and high Induced Polarization (IP) can indicate an oil or gas reservoir. The high power transmitter signal can penetrate the overlying formations to detect this oil and gas anomaly directly. The layout comprises of a transmitter synchronized with the receivers. A frequency optimized high power square-wave current is injected into the ground by an electric dipole, allowing Ex (horizontal electric field) and Hz (vertical magnetic field) to be recorded. The KMS array system includes scheduler and synchronization with transmitter to be able to follow any pre-defined transmission and acquisition sequence. TFEM method Current Transmitter Time LOTEM method After He et. al., 2015 Voltage Voltage Receiver E-field Time H-field Time The Long Offset Transient ElectroMagnetics (LOTEM) method is a Transient ElectroMagnetic (TEM) method in which a primary field is generated by a grounded current dipole. The signal transmitted by the dipole consists of a series of alternating step functions that create a collapsing field that in turn induces electric and magnetic fields in the conducting subsurface. Subsurface properties and features at great depth can be deduced by recording these fields at greater and greater distances from the transmitter during the off times. (Strack, 1992 & 1999) 2016 KMS Technologies - KJT Enterprises Inc. V 2.5 Page 8 of 15

10 Using the KMS array system scheduling function and synchronization with multiple transmitters, the system can realize focused TEM applications, which give better volume focusing. The LOTEM method can be applied to any of the following targets: Sub-basalt and sub-salt mapping (Strack and Pandey, 2007). Mapping of thin resistive layers, like hydrocarbons (electric fields). Determining conductive structures, like geothermal anomalies (magnetic fields, MT combined). Focused source EM (Davydycheva and Rykhlinski, 2009). after Martin, 2009 FSEM method The differential Focused Source EM method FSEM (Rykhlinskaya and Davydycheva, 2014; Davydycheva 2016) obtains an equivalent vertical electric field measure. The vertical electric field Ez more sensitive to deep and shallow resistors, than the horizontal electric field, since such structures significantly affect the vertical current flow. It is also possible to measure Ez in shallow vertical boreholes on the Earth surface with the KMS-888 Shallow Borehole Tools. If borehole Ez measurements are unavailable, the FSEM method helps. It allows accurate determination of small vertical leakage of the electric current. On the left the 2D sensitivity volumes for frequency and time domain are shown as a function of receiver-to-transmitter distance. On the right is the focused source EM current flow depicting that the information comes from below the receiver. On the right we have 3D modeling results simulating the response two oil reservoirs at 2 km depth depicted in the bottom. Frequency and time domain show anomalies between 10-40% while the FSEM anomaly is % KMS Technologies - KJT Enterprises Inc. V 2.5 Page 9 of 15

11 Application history - references Since 2010, the system has been used in: Argentina, Azerbaijan, China, Germany, Kenya, India, Indonesia, Israel, Italy, Saudi Arabia, Slovakia, Thailand, Ukraine, and USA (CA, CO, HI, NV, and TX). Applications include magnetotellurics, Audio-magnetotellurics, Lotem, microseismics (intrusion monitoring), bottom hole-to-surface communication, marine CSEM. Please check our website for an update list of publications using our system: Patents: the system and methods are covered by various patents see our website for the latest list Strack, K. -M., 2003, Integrated borehole system for reservoir detection and monitoring, US & US Strack, K. -M., 2004, Surface and borehole integrated electromagnetic apparatus to determine reservoir fluid properties, US Strack, K.M., Thomsen, L. A., and Rueter, H., 2007, Method for acquiring transient electromagnetic survey data, US Strack, K. M., Rueter, H., and Thomsen, L., 2008, Integrated earth formation evaluation method using controlled source electromagnetic survey data and seismic data, US Strack, K.M., 2009, Method for combined transient and frequency domain electromagnetic measurements, US Rykhlinskaya, E., and Davydycheva, S., 2014, Method for marine geoelectrical exploration with electrical current focusing, U.S. Patent 8,762,062 B2. Davydycheva, S., 2016, Method and apparatus for detecting and mapping subsurface anomalies, U.S. Patent Application US2016/ A1. Jiang, J., Aziz, A.A., Liu, Y., and Strack. K.M., 2015, Geophysical acquisition system, US 9,057,801. References: Buehnemann, J., Henke, C.H., Mueller, C., Krieger, M.H., Zerilli, A., and Strack, K.M., 2002, Bringing complex salt structures into focus - a novel integrated approach: 72nd Annual Meeting, Society Exploration Geophys. Expanded abstracts. Colombo, D., Dasgupta, S., Strack, K.M., and Yu, G., 2010, Feasibility study of surface-to-borehole CSEM for oil-water fluid substitution in Ghawar field, Saudi Arabia: Geo 2010, poster. Davydycheva, S., and Rykhlinski, N., 2009, Focused-source EM survey versus time-domain and frequency-domain CSEM: The Leading Edge, 28, Davydycheva, S., and Rykhlinski, N.I., 2011, Focused source electromagnetic survey versus standard CSEM: 3D modeling in complex geometries, Geophysics, 76, no.1, F27-F41. Davydycheva, S., Kaminsky, A., Rykhlinski, N., and Yakovlev, A., 2015, A large-scale field study in Eastern Siberia using novel time-domain electromagnetic technology, Interpretation, Interpretation, 3, No.2, T109-T120 He, Z., Yu, G., Cheng, H., Wang, Z. Quin, J., and Meng, Y. 2015, Drilling risk assessment through joint EM and seismic data integrated interpretation, Society Expl. Geophys., GEM Chengdu 2015: International Workshop on Gravity, Electrical & Magnetic Methods and Their Applications Chengdu, China. Hu, W., Yan, L., Su, Z., Zheng, R., and Strack, K.M.,2008, Array TEM Sounding and Application for reservoir monitoring: SEG Las Vegas Annual Meeting, Martin, R., 2009, Development and application of 2D and 3D transient electromagnetic inverse solutions based on adjoint Green functions: A feasibility study for spatial reconstruction of conductivity distributions by means of sensitivites, Dissertation, Inst. f. Geophysics & Meteorology, University of Cologne, 213 pp. Passalacqua, H., 1983, Electromagnetic fields due to a thin resistive layer: Geophysical Prospecting, 31, Strack, K.-M., Hanstein, T., Lebrocq, K., Moss, D.C., Petry, H.G., Vozoff, K., and Wolfgram, P.A., 1989, Case histories of LOTEM surveys in hydrocarbon prospective areas: First Break, 7, Strack, K.-M., 1992, Exploration with deep transient electromagnetics, Elsevier, 373 pp. (reprinted 1999) Strack, K.M., and Vozoff, K., 1996, Integrating long-offset transient electromagnetics (LOTEM) with seismics in an exploration environment: Geophysical Prospecting, 44, Strack, K.-M., and Pandey, P.B., 2007, Exploration with controlled-source electromagnetics under basalt covers in India: The Leading Edge, 26, Strack, K.M., 2010, Advances in electromagnetics for reservoir monitoring: Geohorizons, June 2010, Strack, K.-M., 2014, Future directions of Electromagnetic Methods for Hydrocarbon Applications, Surveys in Geophysics, 35, KMS Technologies - KJT Enterprises Inc. V 2.5 Page 10 of 15

12 >15 years of advanced Electromagnetic (EM) methods for the Oil & Gas and Geothermal industries KMS Technologies provides hardware, software and services Product overview - hardware KMS Array acquisition unit for MT, CSEM & microseismics KMS Channel expansion module KMS High power CSEM transmitter (100, 150, 200 KVA) KMS 870-4C seismic & EM deep water marine node EM sensors Induction coils Electrodes Fluxgate magnetometers Product overview - software 3D modelling Acquisition & acquisition QC Data processing 2016 KMS Technologies KJT Enterprises Inc KMS Technologies Product applications Providing the full product range for all electromagnetic (EM) applications Land and Marine Controlled Source EM (CSEM) Land and Marine Magnetotellurics (MT) EM & microseismic reservoir monitoring Geothermal Tel.: USA Fax info@kmstechnologies.com ~200 channel EM and microseismic reservoir monitoring system. Delivered Q Services Feasibility studies Custom R&D projects Boutique acquisition services Product development & manufacture Hardware Software KMS Technologies KJT Enterprises Inc Katy Freeway Suite 200 Houston, Texas Tel.: USA Fax info@kmstechnologies.com Offices in Germany, Thailand & Ukraine 2016 KMS Technologies - KJT Enterprises Inc. V 2.5 Page 11 of 15

13 Electromagnetic sensors LEMI sensors Fluxgate magnetometers: Induction coils: LEMI-011 LEMI-017 LEMI-018 LEMI-118 LEMI-120 LEMI-019 LEMI-020 LEMI-024 LEMI-121 LEMI-123 LEMI-025 Electrodes: LEMI-701 LEMI-029 LEMI-035 Applications: Land & marine CSEM Marine magnetotellurics Land magnetotellurics Permanent sensors Airborne sensors LEMI-142 LEMI-145 LEMI-030 High quality electromagnetic sensors Fluxgate magnetometers: LEMI-011 Low power 3-components fluxgate magnetometer. Frequency (DC-20 Hz) LEMI-017 Autonomous Meteomagnetic station with 7 channels. Frequency (DC-0.3 Hz) LEMI-018 Vector magnetometer for the precise measurements of Earth magnetic field with several sensor options. LEMI-019 Ultra-low power fluxgate featuring two analog outputs: filtered ( Hz) & unfiltered (DC-15 Hz) LEMI-020 Smallest volume compensated fluxgate sensor, with low non-orthogonality, low noise, high resolution. Frequency (DC-100 Hz). LEMI-024 Low power 3-components & highly sensitive analog fluxgate magnetometer. Frequency ( Hz) LEMI-025 Fluxgate magnetometer for super stable measurements of 3-component Earth magnetic field with new 1-second INTERMAGNET. The only commercially available product in this class. Frequency (DC-3.5 Hz) LEMI-029 Low noise fluxgate magnetometer with exceptional low-frequency stability. Frequency (DC-180 Hz) LEMI-035 High resolution and precision low noise magnetometer with both digital and analog outputs. Frequency (DC-20 Hz) Induction coils: LEMI-118 High frequency induction coil (1-70 khz) LEMI-120 Broadband induction coil ( khz) with the lowest noise in class. LEMI-121 Low power, very low noise & compact. Frequency ( Hz), marine EM LEMI-123 Low noise, low power & compact. Frequency (1 Hz -1 khz), high frequency marine EM LEMI-030 Three magnetometers with communication unit, intended for study of magnetic field fluctuations. Frequency ( Hz) LEMI-142 High sensitive magnetometer with low noise Frequency (1 500 khz) LEMI-145 Extremely low noise, low power & lightweight. Frequency ( ,000 Hz) Electrodes: LEMI-701 Ultra-low noise non-polarizable electrodes (Cu-CuSO 4 ), matched pairs KMS Technologies KJT Enterprises Inc Katy Freeway Suite 200 Houston, Texas Tel.: USA Fax info@kmstechnologies.com Offices in Germany, Thailand & Ukraine 2016 KMS Technologies - KJT Enterprises Inc. V 2.5 Page 12 of 15

14 Array acquisition unit for MT & microseismic KMS 820 Product features Low-power design for long recording time Long-range wireless WIFI Bandwidth : DC - 50 khz Up to 80 khz sampling rate Six 24-bit GPS synchronized channels With 32-bit remote acquisition controller Unlimited digital channels expansion Low noise & low drift input amplifiers Portable & lightweight Ruggedized design for field application Acquisition & monitoring software included Processing software for MT & CSEM Low cost Electromagnetic / microseismic data acquisition unit Product applications Land ElectroMagnetics (EM) Acquisition: Magnetotellurics (MT), Lotem, CSAMT, Induced Polarization EM transmitter controller System response recording (time domain) EM survey in array configuration Marine EM Transition zone transmitter & monitor Source controller & environmental monitor (current & one field component) Marine EM version Land seismic Special high bandwidth applications Passive microseismic monitoring for regional & local seismic activities Seismic security surveillance General lab measurement General acquisition system Electrode long term stability Custom versions available KMS Technologies KJT Enterprises Inc Katy Freeway Suite 200 Houston, Texas Tel.: USA Fax info@kmstechnologies.com Offices in Germany, Thailand & Ukraine 2016 KMS Technologies - KJT Enterprises Inc. V 2.5 Page 13 of 15

15 KMS-5100 CSEM transmitter Product features Maximum output: 100, 150 or 200 kva GPS synchronized timing control Long-range wireless for remote control & monitoring Linear ramp better than 5 µs turn off characteristic Bi-polar reversing ramp time < 20 µs Suitable for Time domain EM (TDEM or LOTEM), Induced polarization (IP), TFEM, FSEM etc Target depth of 600 m or deeper Ideal for deep EM geophysical applications 2-4 km Grounded dipole or loop source Integrated in KMS array system via KMS-820-T Controller has 6 analog & (unlimited) digital channels Ruggedized design for field operations Data is saved to SD card (16-32 GB) 150 kva 100 kva Product specifications KMS-5100 Grounded dipole transmitter Current waveform Reversing polarity square (100% duty cycle) or bipolar with off-time (firmware selectable from Hz to 1000 Hz). Other waveform can be generated by controller Transmitter type Dipole source or loop source Maximum output current Maximum output voltage Limited to 125 A unipolar, 250 A bi-polar (100 kva version) Limited to 175 A unipolar, 350 A bi-polar (150 kva version) Limited at 240 A unipolar, 480 A bipolar (200 kva version) 1000 V Output measurement Dimensions 24 bit KMS-820 with KMS-831 up to 32-bit KMS : 0.7 m x 0.9 m x 1.01 m (W x H x D) (14U) Input voltage Frequency range Current recording sampling rate VAC at 50/60 Hz khz < 80 khz, same as receiver acquisition sampling-rate Operating environment Weight -20 C to 50 C -35 C to 50 C (storage) KMS-5100: 30 kg (switchbox only), for 150 kva = 90 kg and 200 kva = 120 kg. Maximum power output 100/150/200 kva at 25 C Duty cycle 100%, 50 %, 33%, 25%, variable User interface Long range wireless, , USB, cable or USB Standard packaging Unit in field container shipped in ruggedized large transport container KMS Technologies KJT Enterprises Inc Katy Freeway Suite 200 Houston, Texas Tel.: USA Fax info@kmstechnologies.com Offices in Germany, Thailand & Ukraine 2016 KMS Technologies - KJT Enterprises Inc. V 2.5 Page 14 of 15

16 Past clients Aramco Saudi Arabia, Anadarko Texas, Apache Texas, Baker Hughes (US & Europe), British Geological Survey - UK, BP Texas, CGG Mexico, Chevron California, CNPC China, ConocoPhillips- Texas, EMGS- Norway, EMI California, GDC Kenya, Geokinetics, ENI Italy, Geosystems Italy, ION, Mannvit Iceland, ORMAT Nevada, PDO Oman, PTTEP Thailand, OMV Austria, Petroalliance Russia, Oyo-Geospace Texas, Philips Oklahoma, RXT Norway, RWE- DEA Germany, Schlumberger Technology Corporation - Texas, Shell Texas, Sinopec- China, Welldynamics Texas, WINS ASA Norway, Wintershall (Germany & Libya) Hardware sales in > 20 countries Research organizations in: Australia, China, Germany, India, Indonesia, Malaysia, Mexico, Thailand, USA (TX, CA, CO, LA, OK, MA, NH, NM, NV) Katy Freeway Suite 200 Houston, Texas USA Phone: info@kmstechnologies.com Worldwide offices: USA, Germany, Thailand & Ukraine KMS Technologies - KJT Enterprises Inc KMS Technologies - KJT Enterprises Inc. V 2.5 Page 15 of 15

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